This document discusses construction of buildings in seismic areas and provides guidelines for earthquake-resistant construction. It defines seismic belts as areas where earthquakes occur frequently and shield areas where they occur rarely or mildly. It recommends that buildings be founded on hard bedrock and avoid irregular shapes, loose soils, or cuttings. Reinforced concrete should be used with raft foundations and all parts of the building well-tied together to act as a single unit during vibrations. The document also discusses the Richter scale for measuring earthquake magnitudes and the increased damage radii from magnitude 5 to 8 earthquakes.
2. SEISMIC BELTS AND SHIELD AREAS:
• Seismic belts are those places where earthquakes occur frequently.
Shield areas are those places where earthquakes occur either rarely or
very mildly.
• Occurrence of an earthquake in a place is an indication of underground
instability there.
• Statistics have revealed that nearly 50% of earthquakes have occurred
along mountain ridges and 40% of earthquakes along steep coasts.
• The study of recorded earthquakes shows that they take place on land
most frequently along two well-defined seismic belts.
1. Circum Pacific Belt which accounts for 68% of earthquake occurrence.
2. Mediterranean belt accounts 21% of earthquake which extends east-west
from Portugal, Himalayas and Burma with a branch through Tibet and
China.
4. RICHETER SCALE:
• The Richter magnitude scale (also Richter scale) assigns a
magnitude number to quantify the energy released by an earthquake.
• The Richter scale, developed in the 1930s, is a base-10 logarithmic
scale, which defines magnitude as the logarithm of the ratio of
the amplitude of the seismic waves to an arbitrary, minor amplitude.
• In 1935, the seismologists Charles Francis Richter and Beno
Gutenberg, of the California Institute of Technology, developed the
(future) Richter magnitude scale, specifically for measuring
earthquakes in a given area of study.
• The Richter scale was succeeded in the 1970s by the Moment
Magnitude Scale (MMS). This is now the scale used by the United
States Geological Survey to estimate magnitudes for all modern large
earthquakes.
6. • An Earthquake of magnitude 5 may cause damage within radius of
8km, but that of magnitude 7 may cause damage in a radius of 80km,
and that of 8 over a radius of 250km.
7. Construction of Buildings in seismic areas- Precautionary
Measures:
• Buildings should be Founded on hard bedrock only and never on
loose soils or Fractured rocks, this is because loose ground settles due
to earthquake vibrations.
• Buildings situated in cuttings on hill slides, near sheet slopes always
suffer more when an earthquake occurs.
• For large Buildings, raft types of foundations are desirable. Square
foundations are more stable.
9. • Different parts of a building should be well tied together so that the
whole structure behaves like a single unit to the Vibrations.
• Only rich cement mortar and reinforced concrete should be used.
• Buildings with irregular shapes with wings, Verandas, Porches and all
structures should be avoided.
• Buildings should have RCC roofs and they should be designed not to
yield to lateral stress.
• Resonance is the important factor, If the period of vibration of a
structure is the same as that of the foundation rock it will collapse
because of the resonance effect.
10. CIVIL ENGINEERING CONSIDERATIONS IN
SEISMIC AREAS:
• Seismic areas are the places which experience
earthquakes frequently.
• Therefore constructions in seismic and
aseismic areas differ in terms of their design.
• So a civil engineer should only think of making
his constructions immune to earthquakes.
11. It is possible to find the difficulties by predicting some crucial
factors:
I. The exact place of earthquake occurrence.
II.The duration of the earthquake.
III.The direction of movement of the ground at the time of
earthquake.